Meteorological history | |
---|---|
Formed | August 26,2016 |
Dissipated | September 2,2016 |
Category 4 hurricane | |
1-minute sustained (SSHWS/NWS) | |
Highest winds | 130 mph (215 km/h) |
Lowest pressure | 950 mbar (hPa);28.05 inHg |
Overall effects | |
Fatalities | None |
Damage | Minimal |
Areas affected | Hawaii |
IBTrACS / [1] | |
Part of the 2016 Pacific hurricane season |
Hurricane Madeline was the first of two tropical cyclones that threatened to make a landfall on Hawaii as a hurricane in 2016,the other being Hurricane Lester. The fourteenth named storm,eighth hurricane and fifth major hurricane of the 2016 Pacific hurricane season,Madeline developed out of an area of low pressure that formed well to the south-southwest of Baja California. By August 26,the disturbance developed to a tropical depression,before becoming a tropical storm shortly afterwards. Wind shear initially inhibited development,however as the cyclone turned northwest,Madeline underwent rapid intensification as an eye feature developed within the storm on August 29. Madeline ultimately peaked as a Category 4 major hurricane the next day. The hurricane then began to weaken as wind shear began to increase as it approached Hawaii. By September 1,Madeline weakened to a tropical storm and passed just south of the Big Island of Hawaii,dumping heavy rainfall,surf,and gusty winds to the island. The cyclone eventually degenerated into a remnant low on September 2 before dissipating later that day.
In advance of both Madeline and Lester to its east,the state of Hawaii began to prepare for a potentially historic strike,possibly two,as the hurricanes approached. Hurricane warnings were issued for the Big Island in preparation for the imminent landfall. As Madeline approached,somewhat weaker than expected,a state of emergency was declared for the entire state of Hawaii still,with dozens of emergency shelters opening on the Big Island. Public schools were closed through September 1 due to the hurricane,and officials advised to stay off any roads and remain indoors if possible. Madeline brought less damage then expected,mainly due to its southward jog and missing the state as a tropical storm,however,areas of Hawaii still experienced heavy rainfall,flooding,storm surge and gusty winds at times.
On August 22, the National Hurricane Center began to monitor a broad area of low pressure that formed about 1,000 mi (1,600 km) south-southwest of the southern tip of Baja California. [2] Over the next few days, the disturbance gradually organized as it tracked westward across the Pacific. Thunderstorm activity increased early on August 25, [3] and as the disturbance further coalesced into the following day, it is estimated that Tropical Depression Fourteen-E formed at 18:00 UTC on August 26, about 1,125 miles (1,811 km) east-southeast of the Big Island of Hawaii. [1] Convective banding features formed to the west of the cyclone, and the depression was later upgraded to Tropical Storm Madeline at 00:00 UTC on August 27. Moving northwestwards under the influence of being located at the southwestern periphery of a mid-level ridge, Madeline strengthened slowly in an environment of moderate wind shear, before crossing 140°W and entering the Central Pacific basin at 00:00 UTC on August 28, at which point the power of issuing advisories on tropical cyclone was transferred to the Central Pacific Hurricane Center. [1]
Once in the Central Pacific, Madeline changed little in intensity until 03:00 UTC on August 29, at which point Madeline began to undergo a period of rapid intensification as an eye feature developed in an organizing central dense overcast (CDO), and it was upgraded to a hurricane at 09:00 UTC that day. [4] Fueled by warm sea surface temperatures in excess of 27 °C (81 °F) and low wind shear, Madeline continued to rapidly strengthen, and by 21:00 UTC, it became a major hurricane – the fifth of the season. [5] The hurricane reached its peak intensity as a powerful Category 4 hurricane at 06:00 UTC the next day with winds of 130 mph (210 km/h) and a minimum pressure of 950 millibars (28 inHg). [1] By later that day, however, the cloud presentation of Madeline began to degrade as wind shear increased slightly due to an upper-level trough that was located near Hawaii, and by mid-day on August 30, as shown by an Air Force reconnaissance aircraft, the hurricane fell below major hurricane intensity by early on August 31 as it approached Hawaii. [6] Further weakening occurred and six hours later it had weakened to a Category 1 hurricane. [7] The eye later disappeared from satellite and reconnaissance data indicated that the low and mid-level centers were beginning to become elongated. [8] Later that day, the circulation became exposed from the convection as wind shear continued to impact the cyclone, and it eventually weakened to a tropical storm by early on September 1. [9] The deepest convection was pushed to the northeast of the center. Despite favorable sea surface temperatures, the wind shear continued to take its toll on Madeline, and although a new burst of convection over the center flared, [10] the tropical storm continued to further deteriorate in structure. Eventually, by late on September 2, Madeline opened up into a trough of low pressure south-southwest of Hawaii. [1]
As Madeline rapid intensified on August 29, posing a great threat to Hawaii, a hurricane watch was issued for Hawaii County. [11] A tropical storm warning and a tropical storm watch was issued for Hawaii County and Maui County respectively on the next day as Madeline moved closer to Hawaii. [12] The CPHC issued a hurricane warning for Hawaii County later that day, the first since Iselle in 2014. [13] The watches in Maui County was modified to tropical storm warning on August 31. [14] The hurricane warning was lowered to tropical storm warning later that day as Madeline weakened and failed to make a landfall in the state. [15] All warnings were discontinued on September 1 as Madeline weakened and moved away from the islands. [16]
Governor of Hawaii David Ige declared a state of emergency on August 30 as Madeline approached, subsequently citing that an emergency relief period be in effect from August 31 to September 9, in preparation of a possible impact from Hurricane Lester. [17] [18] More than a dozen emergency shelters were opened by the American Red Cross of Hawaii to offer food, water and other essential supplies. [19] All public schools were closed on the Big Island through September 1 as Madeline approached. [20] Residents were also strongly advised to stay inside during the storm. [21] The Umauma Bridge (Route 19) was closed in both directions in anticipation of high winds impacting the bridge. [22]
Although Madeline did affect the Big Island, it did not make the major landfall that was anticipated by some meteorologists. Instead, a southwards jog of the system caused much less impacts then what were actually anticipated. Still, Madeline produced heavy rain and gusty winds on the Big Island. In multiple locations, wind gusts exceeded 40 mph (64 km/h), the highest reported being in Waimea, which recorded a peak gust of 60 mph (97 km/h). [23] Total rainfall accumulations amounted up to 5–11 inches (13–28 centimetres) across the Big Island. A few low-lying, flood-prone roads in Hilo were inundated briefly but no significant damages were reported. [24]
Hurricane Jimena was a strong tropical cyclone that brushed Hawaii in early September 2003. It was the tenth named storm and second hurricane of the 2003 Pacific hurricane season. Jimena formed on August 28 in the far Eastern Pacific Ocean as a tropical depression and moved westward where it rapidly became a hurricane the following day. The storm moved westward into the Central Pacific Ocean where it became a Category 2 hurricane on the Saffir–Simpson Hurricane Scale. After reaching its peak strength as a Category 2 hurricane, the storm began to weaken due to increasing wind shear. Jimena brushed past the Hawaiian Islands before becoming a tropical depression on September 3. The weakening storm then crossed the international dateline before dissipating on September 5, becoming one of the few storms to cross both 140ºW and International Date Line.
Hurricane Dora was one of few tropical cyclones to track across all three north Pacific basins and the first since Hurricane John in 1994. The fourth named storm, third hurricane, and second major hurricane of the 1999 Pacific hurricane season, Dora developed on August 6 from a tropical wave to the south of Mexico. Forming as a tropical depression, the system gradually strengthened and was upgraded to Tropical Storm Dora later that day. Thereafter Dora began heading in a steadily westward direction, before becoming a hurricane on August 8. Amid warm sea surface temperatures and low wind shear, the storm continued to intensify, eventually peaking as a 140 mph (220 km/h) Category 4 hurricane on August 12.
Hurricane Flossie was a powerful Pacific tropical cyclone that brought squally weather and light damage to Hawaii in August 2007. The sixth named storm, second hurricane, first and only major hurricane of the inactive 2007 Pacific hurricane season, Flossie originated from a tropical wave that emerged off Africa on July 21. After traversing the tropical Atlantic, the wave crossed Central America and entered the eastern Pacific on August 1. There, a favorable environment allowed it to become a tropical depression and a tropical storm shortly thereafter on August 8.
The 2014 Pacific hurricane season was the fifth-busiest season since reliable records began in 1949, alongside the 2016 season. The season officially started on May 15 in the East Pacific Ocean, and on June 1 in the Central Pacific; they both ended on November 30. These dates conventionally delimit the period of each year when most tropical cyclones form in the Pacific basin.
The 2015 Pacific hurricane season is the second-most active Pacific hurricane season on record, with 26 named storms, only behind the 1992 season. A record-tying 16 of those storms became hurricanes, and a record 11 storms further intensified into major hurricanes throughout the season. The Central Pacific, the portion of the Northeast Pacific Ocean between the International Date Line and the 140th meridian west, had its most active year on record, with 16 tropical cyclones forming in or entering the basin. Moreover, the season was the third-most active season in terms of accumulated cyclone energy, amassing a total of 290 units. The season officially started on May 15 in the Eastern Pacific and on June 1 in the Central Pacific; they both ended on November 30. These dates conventionally delimit the period of each year when most tropical cyclones form in the Northeast Pacific basin. However, the formation of tropical cyclones is possible at any time of the year. This was shown when a tropical depression formed on December 31. The above-average activity during the season was attributed in part to the very strong 2014–16 El Niño event.
The 2016 Pacific hurricane season was tied as the fifth-most active Pacific hurricane season on record, alongside the 2014 season. Throughout the course of the year, a total of 22 named storms, 13 hurricanes and six major hurricanes were observed within the basin. Although the season was very active, it was considerably less active than the previous season, with large gaps of inactivity at the beginning and towards the end of the season. It officially started on May 15 in the Eastern Pacific, and on June 1 in the Central Pacific ; they both ended on November 30. These dates conventionally delimit the period of each year when most tropical cyclones form in these regions of the Pacific Ocean. However, tropical development is possible at any time of the year, as demonstrated by the formation of Hurricane Pali on January 7, the earliest Central Pacific tropical cyclone on record. After Pali, however, no tropical cyclones developed in either region until a short-lived depression on June 6. Also, there were no additional named storms until July 2, when Tropical Storm Agatha formed, becoming the latest first-named Eastern Pacific tropical storm since Tropical Storm Ava in 1969.
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